Water Density Equation:
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The water density equation calculates how water density changes with temperature and pressure. It accounts for thermal expansion (β) and isothermal compressibility (κ) effects on water's density.
The calculator uses the water density equation:
Where:
Explanation: The equation accounts for density changes due to both temperature (thermal expansion) and pressure (compressibility) effects.
Details: Accurate water density calculation is crucial for fluid dynamics, hydrology, oceanography, engineering applications, and scientific experiments where precise density measurements are needed.
Tips: Enter all values in appropriate units. Default values are provided for standard conditions (20°C, 1 atm). Reference density is typically 998.2 kg/m³ for fresh water at 20°C.
Q1: What are typical values for β and κ?
A: For water at 20°C, β ≈ 0.000214 /°C and κ ≈ 4.6×10⁻¹⁰ /Pa. These vary slightly with temperature and pressure.
Q2: How does temperature affect water density?
A: Water density decreases with increasing temperature (above 4°C) due to thermal expansion. Water is unique in having maximum density at 4°C.
Q3: How does pressure affect water density?
A: Increased pressure slightly increases water density due to compression, though water is relatively incompressible compared to gases.
Q4: What's the density of seawater?
A: Seawater is denser (≈1025 kg/m³) due to dissolved salts. This calculator is for pure water. For seawater, salinity must be considered.
Q5: When is this calculation most important?
A: In precise hydrologic measurements, deep ocean studies, high-pressure systems, and temperature-sensitive experiments where small density changes matter.